Groundwater hydrochemistry of Rajnandgaon district, Chhattisgarh, Central India

被引:25
|
作者
Yadav, Ankit [1 ]
Nanda, Abhishek [1 ]
Sahu, Bharat Lal [2 ]
Sahu, Yaman Kumar [3 ]
Patel, Khageshwar Singh [3 ]
Pervez, Shamsh [3 ]
Gulgundi, Mohammad Shahid [4 ]
Cuchi-Oterino, Jose A. [5 ]
Martin-Ramos, Pablo [5 ]
Bhattacharya, Prosun [6 ]
机构
[1] Pt Ravishankar Shukla Univ, Sch Studies Environm Sci, Raipur 492010, CG, India
[2] Guru Ghasidas Cent Univ, Dept Chem, Bilaspur 495009, CG, India
[3] Pt Ravishankar Shukla Univ, Sch Studies Chem, Raipur 492010, CG, India
[4] Presidency Univ, Dept Civil Engn, Bangalore 560064, Karnataka, India
[5] Univ Zaragoza, Inst Invest Ciencias Ambientales IUCA, Dept Agr & Environm Sci, EPS, Carretera Cuarte S-N, Huesca 22071, Spain
[6] KTH Royal Inst Technol, Dept Sustainable Dev Environm Sci & Engn, KTH Int Groundwater Arsen Res Grp, Teknikringen 10B, SE-10044 Stockholm, Sweden
关键词
APCS-MLR; Aquifer; Fluoride; PCA; Seonath river; Source apportionment; FLUORIDE CONTAMINATION; SOURCE APPORTIONMENT; POLLUTION SOURCES; WATER-POLLUTION; PRADESH; RIVER; DISSOLUTION; QUALITY;
D O I
10.1016/j.gsd.2020.100352
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The spreading of fluorosis diseases in Central India related to high concentrations of fluoride ion (F-) is a cause of major concern. In this work, the hydrochemistry of the aquifers related to Seonath River, in Rajnandgaon district, Chhattisgarh state, India, has been studied, focusing on the presence and sources of F-. Hydrochemical parameters were analyzed in the post-monsoon season in 160 wells located in nine tehsils, finding F- concentrations ranging from 0.6 to 18.5 mg L-1. Seasonal variations were also studied in Chhuikhadan tehsil, in which the highest F- values were registered, finding a noticeable enrichment in the pre-monsoon months. In many locations of the district, F- concentrations exceeded the recommended value of 1.5 mg L-1, which have led to the appearance of several health issues. Multidimensional analysis statistical methods were adopted to investigate the sources of F-, and the mineralization of bedrock elements into the groundwater was observed to be the primary source.
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页数:9
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